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Evolution and Understanding of the D-Block Elements in the Periodic Table Cite This: Dalton Trans., 2019, 48, 9408 Edwin C
Dalton Transactions View Article Online PERSPECTIVE View Journal | View Issue Evolution and understanding of the d-block elements in the periodic table Cite this: Dalton Trans., 2019, 48, 9408 Edwin C. Constable Received 20th February 2019, The d-block elements have played an essential role in the development of our present understanding of Accepted 6th March 2019 chemistry and in the evolution of the periodic table. On the occasion of the sesquicentenniel of the dis- DOI: 10.1039/c9dt00765b covery of the periodic table by Mendeleev, it is appropriate to look at how these metals have influenced rsc.li/dalton our understanding of periodicity and the relationships between elements. Introduction and periodic tables concerning objects as diverse as fruit, veg- etables, beer, cartoon characters, and superheroes abound in In the year 2019 we celebrate the sesquicentennial of the publi- our connected world.7 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. cation of the first modern form of the periodic table by In the commonly encountered medium or long forms of Mendeleev (alternatively transliterated as Mendelejew, the periodic table, the central portion is occupied by the Mendelejeff, Mendeléeff, and Mendeléyev from the Cyrillic d-block elements, commonly known as the transition elements ).1 The periodic table lies at the core of our under- or transition metals. These elements have played a critical rôle standing of the properties of, and the relationships between, in our understanding of modern chemistry and have proved to the 118 elements currently known (Fig. 1).2 A chemist can look be the touchstones for many theories of valence and bonding. -
Hjalmar Fors, the Limits of Matter—Chemistry, Mining & Enlightenment
Miner Econ (2015) 28:131–132 DOI 10.1007/s13563-015-0071-2 BOOK REVIEW Hjalmar Fors, The Limits of Matter—Chemistry, mining & enlightenment The University of Chicago Press Chicago USA 2015 Magnus Ericsson1 Published online: 15 September 2015 # Springer-Verlag Berlin Heidelberg 2015 Swedish chemists have discovered more elements than scien- though at that time not united into one yet), France and tists from any other nation. Over more than 100 years, from England? Part of the answer is surprisingly bureaucratisation the early 18th century to the end of the 19th century, 20 ele- or the creation of an administrative institution called ments of which 18 metals or non-metals and 2 gases, nitrogen Bergskollegium in Swedish or English Bureau of Mines as and chlorine were independently isolated and described. Some Hjalmar Fors calls it in his new and path-breaking study of these are as follows: The Limits of Matter—Chemistry, mining & enlightenment. Another part is the need of improved processes and better Element Name Year of discovery yields in Swedish mines, which played such a vital role in Cobalt Brandt 1735 the Swedish economy during this period. The Swedish ruling Nickel Cronstedt 1751 groups saw these demands and founded the Bureau of Mines, Manganese Gahn 1774 which acted in several ways to solve problems, that had arisen in the mining industry. R&D in those days was highly Molybdenum Hjelm 1781 applied but nevertheless led to important purely scientific Yttrium Gadolin 1794 results. Tantalum Ekeberg 1802 The Bureau was set up in 1634 based on a predecessor, Cerium Berzelius 1803 which was started already in 1630. -
Spectrophotometric Determination of Praseodymium by 1,4
Arab Journal of Sciences & Research publishing Issue (2), Volume (1) September 2015 ISSN: 2518 - 5780 Spectrophotometric Determination of Praseodymium by 1,4- Dihydroxyanthraquinone after its Selective Separation from Rosetta Monazite Rare Earth Concentrate by Solvent Extraction Abdel Fattah N. A a Sadeek A. S b Ali B. H a Abdo, A. A a Weheish, H. L.a a Nuclear Materials Authority || Egypt b Faculty of Science || Zagazig University || Egypt Abstract: A rare earths concentrate of Rosetta monazite assays about 44, 23, 16.94 and 5.91 % for Ce, La, Nd and Pr respectively. Separation of cerium by air oxidation at 200oC. Selective separation of Pr by D2EHPA at pH1 followed by a sensitive spectrophotometric method which described for the determination of praseodymium (Pr) with l,4- dihydroxyanthraquinone . The calibration curve was linear from 0.1 to 12 µgml -1 praseodymium. The influences of various parameters and reaction conditions for maximum colour development were investigated. The relative standard deviation for determination of 1 µgml-1 praseodymium has found to be 1.3 after 5 repeated determinations; percent error 5.02%, molar absorptivity (ε) was 1.23x106M-1 cm-1and detection limit was 0.1µgml-1. The method for determination of praseodymium showed good accuracy and selectivity. INTRODUCTION Rare earth elements (REEs), represent one of a set of seventeen chemical elements in the periodic table, specifically the fifteen lanthanides, as well as scandium and yttrium (Connelly, N.G., et al., 2005). It was discovered of the black mineral Gadolinite by Carl Axel Arrhenius in 1787 (Gschneidner, and Cappellen, 1987). Traditionally, the REEs are divided into two groups on the basis of atomic weight; the light REEs are lanthanum through gadolinium (atomic numbers 57 through 64); and the heavy REEs comprise terbium through lutetium (atomic numbers 65 through 71). -
Yttrium Från Ytterby Och Litium Från Utö – Del 1 En Topografisk Karta Stockholm Vid 1200-Talets Slut
Grundämnenas upptäckt Grundämnenas upptäckt Exkursioner till Ytterby och Utö 6-7 juni eller 8-9 juni 6 juni Färje 1371: Strömkajen 08:30 Ytterby 09:30 09:45 – 10:45 Ytterby gruva Buss 682: Ytterby 11:03 Engarn 11:07 Buss 670: Engarn 11:09 Tekniska högskolan 11:44 Buss 4: Östra station 11:52 S:t Eriksplan 12:02 12:15 – 14:00 Rörstrands slott (lunch och visning) 14:00 – 16:00 Birkastan 7 juni Tåg 43: Stockholm City 08:16 Västerhaninge station 08:48 Buss 846: Västerhaninge station 09:09 Årstra brygga 09:22 Färje 2173: Årsta brygga 09:30 Gruvbryggan (Utö) 10:10 10:15 – 14:15 Rävstavik och Utö gruvor (matsäck) Färje 2178: Gruvbryggan (Utö) 14:30 Årsta brygga 15:25 Buss 846: Årstra brygga 15:32 Västerhaninge station 15:50 Tåg 43: Västerhaninge station 15:57 Stockholm City 16:29 Grundämnenas upptäckt Exkursioner till Ytterby och Utö 6-7 juni eller 8-9 juni 8 juni Färje 951: Strömkajen 09:15 Ytterby 10:40 10:55 – 11:45 Ytterby gruva Buss 682: Ytterby 12:03 Engarn 12:07 Buss 670: Engarn 12:09 Tekniska högskolan 12:44 Buss 4: Östra station 12:52 S:t Eriksplan 13:02 13:15 – 15:00 Rörstrands slott (lunch och visning) 15:00 – 17:00 Birkastan 9 juni Tåg 43: Stockholm City 08:16 Västerhaninge station 08:48 Buss 846: Västerhaninge station 09:09 Årstra brygga 09:22 Färje 2173: Årsta brygga 09:30 Gruvbryggan (Utö) 10:10 10:15 – 14:15 Rävstavik och Utö gruvor (matsäck) Färje 2178: Gruvbryggan (Utö) 14:30 Årsta brygga 15:25 Buss 846: Årstra brygga 15:32 Västerhaninge station 15:50 Tåg 43: Västerhaninge station 15:57 Stockholm City 16:29 -
GLOBAL RARE-EARTH PRODUCTION: HISTORY and OUTLOOK History – the Discovery
Center for Strategic and International Studies Rare Earth Elements: Geology, Geography, and Geopolitics James B. Hedrick Hedrick Consultants, Inc. U.S. Rare Earths, Inc. Burke, Virginia December 15, 2010 Washington, DC GLOBAL RARE-EARTH PRODUCTION: HISTORY AND OUTLOOK History – The Discovery . The rare earths were discovered in 1787 by Swedish Army Lieutenant Carl Axel Arrhenius . Carl, an amateur mineralogist collected the black mineral ytterbite, later renamed gadolinite, from a small feldspar and quartz mine at Ytterby, Sweden . With similar chemical structures the rare earths proved difficult to separate . It was not until 1794 that Finnish chemist Johann Gadolin separated the first impure yttrium oxide from the mineral ytterbite History – The Discovery History – The Commercialization . The rare earths were commercialized when the incandescent lamp mantle industry was established in 1884 with mantles of zirconium, lanthanum, and yttrium oxides with later improvements requiring only the oxides of thorium and cerium. The lamp mantle was discovered by Baron Carl Auer von Welsbach . The mantles also used small amounts of neodymium and praseodymium as an indelible brand name Welsbach label History – The Early Mining . Rare earths were first produced commercially in the 1880s with the mining in Sweden and Norway of the rare-earth thorium phosphate mineral monazite . Foreign Production Brazil produced monazite as early as 1887 India produced monazite starting in 1911 . Domestic Production Monazite production in the United States was first recorded in 1893 in North Carolina - a small tonnage of monazite was reportedly mined in 1887 Monazite mining in South Carolina began in 1903 History – The Processing . Three main methods for separating and refining the rare- earth elements since they were discovered . -
RBRC-32 BNL-6835.4 PARITY ODD BUBBLES in HOT QCD D. KHARZEEV in This ~A~Er We Give a Pedawwicalintroduction~0 Recent Work Of
RBRC-32 BNL-6835.4 PARITY ODD BUBBLES IN HOT QCD D. KHARZEEV RIKEN BNL Research Center, Br$ookhauenNational Laboratory, . Upton, New York 11973-5000, USA R.D. PISARSKI Department of Physics, Brookhaven National Laboratoy, Upton, New York 11973-5000, USA M.H.G. TYTGAT Seruice de Physique Th&orique, (7P 225, Uniuersitc4Libre de Bruzelles, B[ud. du !t%iomphe, 1050 Bruxelles, Belgium We consider the topological susceptibility for an SU(N) gauge theory in the limit of a large number of colors, N + m. At nonzero temperature, the behavior of the topological susceptibility depends upon the order of the reconfining phrrse transition. The meet interesting possibility is if the reconfining transition, at T = Td, is of second order. Then we argue that Witten’s relation implies that the topological suscepti~lfity vanishes in a calculable fdion at Td. Ae noted by Witten, this implies that for sufficiently light quark messes, metaetable etates which act like regions of nonzero O — parity odd bubbles — can arise at temperatures just below Td. Experimentally, parity odd bubbles have dramatic signature% the rI’ meson, and especially the q meson, become light, and are copiously produced. Further, in parity odd bubbles, processes which are normally forbidden, such as q + rr”ro, are allowed. The most direct way to detect parity violation is by measuring a parity odd global seymmetry for charged pions, which we define. 1 Introduction In this .-~a~er we give a Pedawwicalintroduction~0 recent work of ours? We I consider an SU(IV) gau”ge t~e~ry in the limit of a large number of colors, N + co, This is, of course, a familiar limit? We use the large N expansion I to investigate the behavior of the theory at nonzero temperature, especially for the topological susceptibility. -
EMD Uranium (Nuclear Minerals) Committee
EMD Uranium (Nuclear Minerals) Committee EMD Uranium (Nuclear Minerals) Mid-Year Committee Report Michael D. Campbell, P.G., P.H., Chair December 12, 2011 Vice-Chairs: Robert Odell, P.G., (Vice-Chair: Industry), Consultant, Casper, WY Steven N. Sibray, P.G., (Vice-Chair: University), University of Nebraska, Lincoln, NE Robert W. Gregory, P.G., (Vice-Chair: Government), Wyoming State Geological Survey, Laramie, WY Advisory Committee: Henry M. Wise, P.G., Eagle-SWS, La Porte, TX Bruce Handley, P.G., Environmental & Mining Consultant, Houston, TX James Conca, Ph.D., P.G., Director, Carlsbad Research Center, New Mexico State U., Carlsbad, NM Fares M Howari, Ph.D., University of Texas of the Permian Basin, Odessa, TX Hal Moore, Moore Petroleum Corporation, Norman, OK Douglas C. Peters, P.G., Consultant, Golden, CO Arthur R. Renfro, P.G., Senior Geological Consultant, Cheyenne, WY Karl S. Osvald, P.G., Senior Geologist, U.S. BLM, Casper WY Jerry Spetseris, P.G., Consultant, Austin, TX Committee Activities During the past 6 months, the Uranium Committee continued to monitor the expansion of the nuclear power industry and associated uranium exploration and development in the U.S. and overseas. New power-plant construction has begun and the country is returning to full confidence in nuclear power as the Fukushima incident is placed in perspective. India, Africa and South America have recently emerged as serious exploration targets with numerous projects offering considerable merit in terms of size, grade, and mineability. During the period, the Chairman traveled to Columbus, Ohio to make a presentation to members of the Ohio Geological Society on the status of the uranium and nuclear industry in general (More). -
Hexagon Fall
Redis co very of the Elements The Rare Earth s–The Beginnings I I I James L. Marshall, Beta Eta 1971 , and Virginia R. Marshall, Beta Eta 2003 , Department of Chemistry, University of North Texas, Denton, TX 76203-5070, [email protected] 1 Rare earths —introduction. The rare earths Figure 1. The “rare earths” are defined by IUPAC as the 15 lanthanides (green) and the upper two elements include the 17 chemically similar elements of the Group III family (yellow). These elements have similar chemical properties and all can exhibit the +3 occupying the f-block of the Periodic Table as oxidation state by the loss of the highest three electrons (two s electrons and either a d or an f electron, well as the Group III chemical family (Figure 1). depending upon the particular element). A few rare earths can exhibit other oxidation states as well; for These elements include the 15 lanthanides example, cerium can lose four electrons —4f15d 16s 2—to attain the Ce +4 oxidation state. (atomic numbers 57 through 71, lanthanum through lutetium), as well as scandium (atomic number 21) and yttrium (atomic number 39). The chemical similarity of the rare earths arises from a common ionic configuration of their valence electrons, as the filling f-orbitals are buried in an inner core and generally do not engage in bonding. The term “rare earths” is a misnome r—these elements are not rare (except for radioactive promethium). They were named as such because they were found in unusual minerals, and because they were difficult to separate from one another by ordinary chemical manipula - tions. -
Evolution and Understanding of the D-Block Elements in the Periodic Table Cite This: Dalton Trans., 2019, 48, 9408 Edwin C
Dalton Transactions View Article Online PERSPECTIVE View Journal | View Issue Evolution and understanding of the d-block elements in the periodic table Cite this: Dalton Trans., 2019, 48, 9408 Edwin C. Constable Received 20th February 2019, The d-block elements have played an essential role in the development of our present understanding of Accepted 6th March 2019 chemistry and in the evolution of the periodic table. On the occasion of the sesquicentenniel of the dis- DOI: 10.1039/c9dt00765b covery of the periodic table by Mendeleev, it is appropriate to look at how these metals have influenced rsc.li/dalton our understanding of periodicity and the relationships between elements. Introduction and periodic tables concerning objects as diverse as fruit, veg- etables, beer, cartoon characters, and superheroes abound in In the year 2019 we celebrate the sesquicentennial of the publi- our connected world.7 Creative Commons Attribution-NonCommercial 3.0 Unported Licence. cation of the first modern form of the periodic table by In the commonly encountered medium or long forms of Mendeleev (alternatively transliterated as Mendelejew, the periodic table, the central portion is occupied by the Mendelejeff, Mendeléeff, and Mendeléyev from the Cyrillic d-block elements, commonly known as the transition elements ).1 The periodic table lies at the core of our under- or transition metals. These elements have played a critical rôle standing of the properties of, and the relationships between, in our understanding of modern chemistry and have proved to the 118 elements currently known (Fig. 1).2 A chemist can look be the touchstones for many theories of valence and bonding. -
From Bedrock to Porcelain a Study Regarding The
Bachelor Thesis Degree Project in Geology 15 hp From Bedrock to Porcelain A study regarding the history of porcelain, Ytterby mine and the discovery of yttrium in Sweden Timmy Kärrström Stockholm 2017 Department of Geological Sciences Stockholm University SE-106 91 Stockholm Sweden Abstract Porcelain is a translucent vitreous material that consists of clay (kaolin), feldspar and quartz which has been mixed and heated together to cause a metamorphic reaction. In Sweden, the Porcelain industry was established in 1726 at Rörstrands castle in Stockholm and is today one of the oldest industries in Europe to produce porcelain. Around the 1790’s Rörstrand got its feldspars and quartz from the Ytterby mine that was located at Resarö in Stockholm’s archipelago making the raw material somewhat easy to access. Rörstrand owned the mine in the 1850’s to 1926. During the time Ytterby mine was active, an amateur geologist by the name of Carl Axel Arrhenius, discovered an unusual black mineral in the quarry ore in 1787 which later led to the discovery of 8 new rare earth elements (REE) with the help of several Swedish chemists throughout time. These elements are Yttrium, Ytterbium, Gadolinium, Terbium, Thulium, Erbium, Holmium and scandium. This study will focus on the Swedish porcelain industry and how it has evolved throughout history and Rörstrand’s role in the discovery of yttrium. PAGE 1 Contents Abstract ........................................................................................................................................... 1 -
Experimental Investigation of Recycling Rare Earth Elements from Waste Fluorescent Lamp Phosphors
EXPERIMENTAL INVESTIGATION OF RECYCLING RARE EARTH ELEMENTS FROM WASTE FLUORESCENT LAMP PHOSPHORS by Patrick Max Eduafo A thesis submitted to the Faculty and the Board of Trustees of the Colorado School of Mines in partial fulfillment of the requirements for the degree of Master of Science (Metallurgical and Material Engineering). Golden, Colorado Date: Signed: Patrick Max Eduafo Signed: Dr. Brajendra Mishra Thesis Advisor Golden, Colorado Date: Signed: Dr. Michael Kaufman Professor and Head Department of Metallurgical & Material Engineering ii ABSTRACT Characterization techniques and experimental measurements were used to evaluate a process for recycling rare earth elements (REEs) from spent fluorescent lamp phosphors. QEMSCAN analysis revealed that 70% of the rare earth bearing minerals was less than 10 µm in size. Feeds of varying characteristic were received throughout the course of the experimental analysis. A representative sample of the as-received feed contained 5.8% total rare earth elements (TREE) and upon sieving to below 44 µm, the grade increased to 16.5% TREE. By sieving further to below 10 µm, the grade increased to 19.8% TREE. Hydrochloric acid was used as lixiviant in batch leach experiments on the phosphor powder. The maximum extraction obtained was 90% for europium and yttrium at the following conditions: 1.5 M HCl, 70˚C, 1 hr, 30 g/L and 200 rpm. However, the solubility of cerium, lanthanum and terbium remained low under these conditions. Multistage leaching and calcination followed by leaching processes also resulted in poor extraction of cerium, lanthanum and terbium. Based on experimental results a new process for extracting the chief REEs from end of life fluorescent lamps has been developed. -
CW Scheele, from Pharmacist's Apprentice to Man of Science
ambix, vol. 55, No. 1, March 2008, 29–49 Stepping through Science’s Door: C. W. Scheele, from Pharmacist’s Apprentice to Man of Science1 HJALMAR FORS Division of History of Science and Technology, Royal Institute of Technology, Stockholm This reinterpretation of Carl Wilhelm Scheele’s (1742–86) early life and career analyses the social interplay between Scheele and other chemists who were active in eighteenth-century Sweden. It is argued that Scheele, a rather lowly journeyman working in peripheral pharmacies, had to work hard and traverse several geographical and social boundaries to gain a foothold in the scientifi c community. Eventually, Scheele’s skilful analysis of the mineral magnesia nigra would establish him as one of the pivotal Swedish chemists. However, this happened only after Scheele had managed to prove himself as a knowledgeable chemist who did not threaten the authority of certain socially superior colleagues. When Scheele had gained a place in the scien- tifi c community, the exchange logic of the eighteenth-century republic of letters permitted him to trade experimental results for other kinds of resources. Hence, he gained in both social status, economic prosperity and scientifi c prominence in a relatively short time. Carl Wilhelm Scheele has been, and still is, the object of much admiration. In biographical texts he is often portrayed as the perfect scientifi c hero: humble begin- nings, miraculous discovery, worldwide fame, and an early death caused by long hours spent working over poisonous substances in a drafty chemical laboratory. The legacy of his short life is said to be the discovery of a great number of chemical 1 This paper is based on chapter 6 in the author’s doctoral thesis Mutual Favours: The Social and Scientifi c Practice of Eighteenth-century Swedish chemistry, Institutionen för idé- och lärdomshistoria: skrifter 30 (Uppsala: Uppsala University, 2003).